arrive late

arrive late的基本解释

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迟到

与arrive late相关的网络例句 [注：此内容来源于网络，仅供参考]

music academics conduct and actions is an academics, it have the system of oneself, from music of many main factor of feeling carnal knowledge arrive reasonableness understanding;from most basically and at a time when"a clap" arrive various note at a time when;arrive to reply beat from the simple time;from basic dance the step arrive action of combination, from shallow go into deep situation step launch, let student practice in operation gradually acquire study plain knowledge and basic technical ability of the music foundation.

音乐学科作为一门学科，它有着自身的体系，从音乐的诸多要素的感性经验到理性认识；从最基本的时值"一拍"到各种音符的时值；从单拍子到复拍子；从基本舞步到动作的组合，由浅入深地步步展开，让学生实践操作中逐步获得学习浅显的音乐基础知识和基本技能。

The tectonic evolution of southern Junggar basin can be classified into seven stages: stage of intracontinental rift from middle Periman to late Late Carboniferous; stage of weak extension and peneplane from late Permian to early Triassic; stable depression stage in middle-late Triassic; maximal basin formation phase in the setting of weak extension in early-middle Jurassic; inactive depressed basin formation phase in thrust setting in middle-late Jurassic; stable depression stage in Cretaceous and Eogene; foreland depressed basin formation phase in thrust setting in Neocene and Quaternary.

准噶尔盆地南缘晚石炭世以来盆地构造演化可划分为七个演化阶段：晚石炭世—中二叠世陆内裂谷作用阶段；晚二叠世到早三叠世处于弱伸展-稳定坳陷作用阶段；中、晚三叠世准平原化作用阶段；早、中侏罗世为弱伸展背景下广盆形成阶段；中、晚侏罗世冲断背景下的坳陷盆地形成阶段；白垩纪到古近纪弱伸展背景下的稳定坳陷盆地形成阶段；新近纪—第四纪为冲断背景下的前陆坳陷盆地形成阶段。

The change of REE composition between the upper and lower samples from Hongcan well implied the tectonic setting and property of the sediment provenance in Zoige Basin were altered obviously between late-period of Middle Triassic and mid-period or late-period of Late Triassic. This change was probably due to elevation and erosion of the matured continental crust on the east of Zoige Basin, and lots of clastic materials transported into the basin in late-period of Late Triassic.

通过对比杂砂岩稀土元素组成在上层和下层样品之间的变化，若尔盖盆地内中三叠世中期到晚三叠世中期及晚期沉积物源区的构造背景和性质发生了明显的改变，而这一变化很可能是盆地东侧成熟陆壳在晚三叠世后期被抬升和剥蚀，其大量碎屑物质被带到盆地的结果。